(UUID : c3b80092-506b-4b09-853a-d5a0886420bb)
Rock
Diopside gneiss
M-047
Rock
metamorphic rock
It was metamorphosed at medium to high temperatures and has a higher degree of metamorphism than schist. Gneissosity is developed. Recrystallization is evident. Foliation is less distinct than that of phyllite. Diopside is characteristically present.
11.0
cm
Quartz, Biotite, Orthoclase, Plagioclase
#metamorphic rock
United States
Idaho
Idaho Co, Lowell
Department of Geology and Geophysics, Kangwon National University
+82-33-250-8550
Igneous Petrology and Ladoratory
DOI
CC BY-NC - The author is free to use, but not for profit.
The copyright of this data is held by KIGAM.
2024-09-05